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Phylogenomics reveals rapid, simultaneous diversification of three major clades of Gondwanan frogs at the Cretaceous–Paleogene boundary Yan-Jie Fenga, David C. Blackburnb, Dan Lianga, David M. Hillisc, David B. Waked,1, David C. Cannatellac,1, and Peng Zhanga,1 aState Key Laboratory of Biocontrol, College of Ecology and Evolution, School of Life Sciences, Sun Yat-Sen University, Guangzhou 510006, China; bDepartment of Natural History, Florida Museum of Natural History, University of Florida, Gainesville, FL 32611; cDepartment of Integrative Biology and Biodiversity Collections, University of Texas, Austin, TX 78712; and dMuseum of Vertebrate Zoology and Department of Integrative Biology, University of California, Berkeley, CA 94720 Contributed by David B. Wake, June 2, 2017 (sent for review March 22, 2017; reviewed by S. Blair Hedges and Jonathan B. Losos) Frogs (Anura) are one of the most diverse groups of vertebrates The poor resolution for many nodes in anuran phylogeny is and comprise nearly 90% of living amphibian species. Their world- likely a result of the small number of molecular markers tra- wide distribution and diverse biology make them well-suited for ditionally used for these analyses. Previous large-scale studies assessing fundamental questions in evolution, ecology, and conser- used 6 genes (∼4,700 nt) (4), 5 genes (∼3,800 nt) (5), 12 genes vation. However, despite their scientific importance, the evolutionary (6) with ∼12,000 nt of GenBank data (but with ∼80% missing history and tempo of frog diversification remain poorly understood. data), and whole mitochondrial genomes (∼11,000 nt) (7). In By using a molecular dataset of unprecedented size, including 88-kb the larger datasets (e.g., ref. 6), most data (>50%) are from the characters from 95 nuclear genes of 156 frog species, in conjunc- 12S and 16S mitochondrial ribosomal genes. The limited tion with 20 fossil-based calibrations, our analyses result in the amount of data also causes a wide range of estimates of di- most strongly supported phylogeny of all major frog lineages and vergence times for many nodes in the tree. For example, age provide a timescale of frog evolution that suggests much younger estimates for the last common ancestor of extant Neobatrachia, divergence times than suggested by earlier studies. Unexpectedly, oftenreferredtoas“modern frogs” and containing 95% of our divergence-time analyses show that three species-rich clades extant anuran species, span ∼100 Mya (5, 7–11). Furthermore, (Hyloidea, Microhylidae, and Natatanura), which together com- divergences time estimates among the earliest neobatrachian prise ∼88% of extant anuran species, simultaneously underwent clades, such as the Heleophrynidae, Myobatrachidae, Calyp- rapid diversification at the Cretaceous–Paleogene (K–Pg) bound- tocephalellidae, Nasikabatrachidae, and Sooglossidae, range ary (KPB). Moreover, anuran families and subfamilies containing from the Late Jurassic to early Cretaceous (∼150–100 Mya) arboreal species originated near or after the KPB. These results and have wide CIs (5, 7–11). In addition to these species-poor – suggest that the K Pg mass extinction may have triggered explo- groups of neobatrachians, there are two species-rich clades: sive radiations of frogs by creating new ecological opportunities. Ranoidea (39% of extant anuran species, mostly Old World) This phylogeny also reveals relationships such as Microhylidae and Hyloidea (54%; mostly New World). The estimated ages being sister to all other ranoid frogs and African continental lineages of Natatanura forming a clade that is sister to a clade Significance of Eurasian, Indian, Melanesian, and Malagasy lineages. Biogeo- graphical analyses suggest that the ancestral area of modern frogs was Africa, and their current distribution is largely associ- Frogs are the dominant component of semiaquatic vertebrate ated with the breakup of Pangaea and subsequent Gondwanan faunas. How frogs originated and diversified has long attrac- fragmentation. ted the attention of evolutionary biologists. Here, we recover their evolutionary history by extensive sampling of genes and amphibia | Anura | nuclear genes | phylogeny | divergence time species and present a hypothesis for frog evolution. In contrast to prior conclusions that the major frog clades were estab- lished in the Mesozoic, we find that ∼88% of living frogs robust, reliable phylogeny is essential to understand the role originated from three principal lineages that arose at the end Aof macroevolutionary processes in generating biodiversity. of the Mesozoic, coincident with the Cretaceous–Paleogene However, resolution of evolutionary relationships among certain (K–Pg) mass extinction event that decimated nonavian dino- groups has been persistently difficult because of sparse genotypic saurs 66 Mya. The K–Pg extinction events played a pivotal role and phenotypic data. Frogs (Anura) are one such example; they in shaping the current diversity and geographic distribution of are one of the most diverse groups of tetrapods, and currently modern frogs. comprise 6,775 described species, 446 genera, and 55 families (1) that are well represented on all continents. They exhibit great Author contributions: D.C.B., D.M.H., D.B.W., D.C.C., and P.Z. designed research; D.C.B., adaptive diversity within a highly constrained phenotype esti- D.M.H., D.B.W., D.C.C., and P.Z. designed and carried out taxon sampling; D.C.B. and mated to be 200 My old. Evolutionary convergence in body form, D.C.C. selected and vetted calibration points; Y.-J.F. and D.L. performed laboratory research; Y.-J.F., D.L., and P.Z. analyzed data; and Y.-J.F., D.C.B., D.L., D.M.H., D.B.W., life history, and behavioral traits is widespread in frogs, including D.C.C., and P.Z. wrote the paper. forms reflecting different microhabitat use by arboreal, aquatic, Reviewers: S.B.H., Temple University; and J.B.L., Harvard University. and fossorial species. These features make frogs a challenging but The authors declare no conflict of interest. fascinating model for addressing fundamental questions of mor- Freely available online through the PNAS open access option. phological, developmental, and biogeographical evolution. How- – Data deposition: The sequences reported in this paper have been deposited in the Gen- ever, despite intensive molecular phylogenetic studies (2 7), areas Bank database. For a list of accession numbers, see Dataset S1. of uncertainty and disagreement persist among clades that are 1 To whom correspondence may be addressed. Email: [email protected], catfish@ crucial for interpreting broad-scale macroevolutionary patterns. utexas.edu, or [email protected]. In addition, a general consensus on divergence times of the major This article contains supporting information online at www.pnas.org/lookup/suppl/doi:10. anuran lineages is also lacking (7, 8). 1073/pnas.1704632114/-/DCSupplemental. E5864–E5870 | PNAS | Published online July 3, 2017 www.pnas.org/cgi/doi/10.1073/pnas.1704632114 Downloaded by guest on October 2, 2021 of each clade range from the Late Jurassic to the end of the Relationships within the Afrobatrachia mirror those found in PNAS PLUS Cretaceous, spanning ∼100 My, and relationships of family-level other studies (5–7, 14). taxa within each clade remain poorly resolved. Natatanura is a large clade of extant anurans (24% of species) In this study, we increased gene sampling by using a recently de- and mainly found in the Old World. Our ML and Bayesian to- veloped nuclear marker toolkit (12). Our new data include ∼88,000 nt pologies of Natatanura are identical. All nodes in the Bayesian of aligned sequences from 95 nuclear protein-coding genes covering tree have a BPP of 1.0, and only three nodes in the ML tree have 164 species (156 anuran species and 8 outgroups) from 44 of 55 frog BSs <90%. The 309-species topology is identical, but with low families; to our knowledge, this is the largest source of new data for support among the deeper branches, likely because of missing anuran phylogenetics. In addition, we enlarged this dataset to a total data. Notably, we found that endemic African continental lineages of 301 anuran species by incorporating previously published (Conrauidae, Odontobatrachidae, Petropedetidae, Phrynoba- RAG1 and CXCR4 sequences so that all 55 extant frog families were trachidae, Ptychadenidae, Pyxicephalidae) form a clade that is included. Our goal was to propose a robust hypothesis of phyloge- the sister group to the clade of the remaining North American, netic relationships and divergence times of the major lineages. Our Eurasian, Melanesian, and Malagasy lineages (Ceratobatrachidae, results resolve previously intractable relationships, generate diver- Dicroglossidae, Mantellidae, Rhacophoridae, and Ranidae; Fig. gence times with narrow CIs, and provide perspectives on the evo- 1A and Figs. S1–S4). This African clade has low bootstrap sup- lutionary history and historical biogeography of frogs. port (56%) but high Bayesian support (1.0). The clade of the remaining non-African families is strongly supported (BS = Results and Discussion 100%), and the internal branches are strongly supported (BS = Data Characteristics. We assembled a de novo 164-species dataset 100%, BPP = 1.0), although they are short. In other studies, this by using 95 nuclear genes (Table S1) and 88,302 nt from 156 frog group of African lineages is not monophyletic (6, 7, 10, 14, 15). species and 8 outgroups; this matrix is 89.6% complete. To increase The phylogenetic position of the continental African lineages has coverage of anuran families, we added sequences of RAG1 and important biogeographic significance (as detailed later). CXCR4 from GenBank of 145 additional anuran species. This Relationships among the subfamilies of Microhylidae (one of 309-species dataset contains 88,386 nt and is 48.2% complete. the largest anuran families, including 8.8% of all species), which The 164-species and 309-species matrices are available from the have significant radiations on most continents and the large is- Dryad Digital Repository (doi:10.5061/dryad.12546). lands Madagascar and New Guinea, have proven difficult to resolve (4, 6, 7, 15–19).